Chapter 2 Flashcards

1
Q

naturally occurring solids •formed by inorganic
processes
•building blocks of rocks •Examples: quartz, sulfides,
halides

A

Minerals

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2
Q

•relatively hard, naturally occurring mineral material
•made up of two of more
minerals, mixed up through
geological processes
• Examples: igneous, sedimentary,
and metamorphic rocks

A

Rocks

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3
Q

Physical Properties of Rock-Forming Minerals

A

Color
Hardness
Luster
Cleavage

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4
Q

it is a measure of the resistance of a mineral (not specifically surface) to abrasion

A

Hardness

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5
Q

measures the scratch resistance of various minerals based on the ability of a harder material/mineral to scratch a softer one

A

The Mohs Scale of Hardness

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6
Q

describes how the mineral reflects light

A

Luster

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7
Q

2 types of luster

A

Metallic luster
Non-metallic luster

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8
Q

looks like a shiny metal such as chrome, steel, silver, or gold.

A

Metallic luster

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9
Q

may be shiny and reflect light, however, they do not look like a metal.

A

Non-metallic luster

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10
Q

the property of some minerals to break along specific planes of weakness to form smooth, flat surfaces.

A

Cleavage

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11
Q

is the property of a mineral breaking in a more or less random pattern with no smooth planar surfaces.

A

Fracture

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12
Q

Cleavage in one direction

A

Muscovite

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13
Q

Cleavage in two directions

A

Feldspar

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14
Q

Cleavage in three directions

A

Halite

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15
Q

Cleavage in four directions

A

Calcite

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16
Q

Mineral Groups

A

Silicates
Oxides
Carbonates
Halides

17
Q

minerals containing the two most abundant elements in the Earth’s crust, namely, silicon and oxygen

A

Silicates

18
Q

minerals composed of oxygen anion (O2-) combined with one or more metal ions

A

Oxides

19
Q

minerals containing the carbonate (CO3)2- anion combined with other elements

A

Carbonates

20
Q

minerals containing halogen elements combined with one or more metal

A

Halides

21
Q

There are almost —— known mineral species, yet the vast majority of rocks are formed from combinations of a few common minerals, referred to as “——————”.

A

5000
Rock-forming minerals

22
Q

are naturally occurring and coherent aggregate of one or more minerals
basic unit of which the solid Earth

A

Rocks

23
Q

3 major types of rocks

A

Igneous, sedimentary, metamorphic

24
Q

those that solidify from magma

A

Igneous rock

25
Q

magma cools quickly above ground (extrusive)

A

Volcanic igneous rock

26
Q

magma cools and solidifies slowly underground (intrusive)

A

Plutonic igneous rock

27
Q

those that are deposited and lithified (compacted and cemented together) at the Earth’s surface

A

Sedimentary

28
Q

compacted broken rocks (sandstone)

A

Clastic

29
Q

compacted dissolved minerals (limestone)

A

Chemical

30
Q

compacted biogenic
matter (coal)

A

Organic

31
Q

is a process that squeezes, or compacts sediments.

A

Compaction

32
Q

“glue” – takes place when dissolved minerals are deposited in the tiny spaces among sediments.

A

Cementation

33
Q

formed by changes in preexisting rocks under the influence of high temperature, pressure, and chemically active solutions

A

Metamorphic rocks

34
Q

2 types of metamorphic rocks

A

Foliated
Non-foliated

35
Q

have a layered or banded appearance

A

Foliated

36
Q

do not have a layered or banded appearance

A

Non-foliated

37
Q

is a web of processes that outlines how each of the three major rock types—igneous, metamorphic, and sedimentary—form and break down based on the different applications of heat and pressure over time.

A

Rock cycle